Abstract

Periglacial activity on Heard Island is manifested by intense physical weathering of the longest-exposed surfaces, and hillslope forms produced
by a variety of cold-climate mass wasting processes. Microrelieffeatures include rudimentary sorted steps, terraces and polygons. No evidence
of deep cryoturbation was obtained from excavations at 14 sites in moraines and no landforms indicative of discontinuous permafrost were
identified. Periglacial landform development has been inhibited by the maritime climate and is more restricted than on other islands in
the region due to the low altitude of the ice-free terrain, limited extent of glacier-free ground, and relatively recent deglaciation.